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Put the water-movement pathway in the most typical order during a prolonged storm on a vegetated slope (track water from the surface into deeper material).

  • Throughflow: water moves laterally downslope within the soil

  • Percolation: water drains downward into deeper material/bedrock fractures/groundwater

  • Infiltration: water enters the soil from the surface

  • Soil-moisture storage increases (soil pores fill)

  • Rainwater reaches the ground surface (after interception is exceeded)

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